advection fog

It can also form due to the lifting of advection fog during breezy conditions.

Spring and fall cold fronts often form advection fog which pushes the marine layer towards the coast.

Advection fog often develops along seacoasts where warm air comes in contact with cold ocean currents.

Most advection fog develops when warm, moist air rides in over a cold surface-land, ice, or water.

Non-frontal low stratiform cloud can form when advection fog is lifted above surface level during breezy conditions.

Sometimes advection fog is formed when a mass of air is forced across rising terrain, such as the slope of a mountain.

Advection fog occurs when moist air passes over a cool surface by advection (wind) and is cooled.

Dense advection fog can form when warm air moves over the cool shelf waters during February and March, stopping ship traffic for days.

There are many types of fog, such as evaporation fog, advection fog, radiation fog, and upslope fog.

The village is practically fog-free; only radiation fog is seen now and then, as well as the odd advection fog inflow from the Hosenbach valley within the framework of a local atmospheric circulation that forms with low-gradient anticyclonic weather systems.

Virtually everyone here is an amateur meteorologist and can speak with authority of micro-climates, prevailing westerlies, pressure systems, currents and the difference between the advection fog here in the Bay Area and the tule fog that closes highways in winter in the San Joaquin Valley.

Judges confirmed that a natural phenomenon called advection fog (a quick buildup of thick fog in a small area caused by hot, moist air reaching the cold sea surface) was experienced that evening in the zone around the Agip Abruzzo, preventing the Moby Prince from spotting the tanker.